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A viscous continuum theory of sea ice motion based on stochastic floe dynamics – CORRIGENDUM

Published online by Cambridge University Press:  23 September 2025

Abstract

Information

Type
Corrigendum
Creative Commons
Creative Common License - CCCreative Common License - BY
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (https://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution and reproduction, provided the original article is properly cited.
Copyright
© The Author(s), 2025. Published by Cambridge University Press

Equation 3.4 as it appears in the main text is incorrect. The correct equation is:

(C3.4) \begin{align} \left (\frac {\partial \mathcal{P}}{\partial t} - \frac {\partial \boldsymbol{u}^{\infty }}{\partial t} \boldsymbol{\cdot }\boldsymbol{\nabla} _{\boldsymbol{v'}} \mathcal{P}\right ) + \left (\boldsymbol{u}^{\infty } + \boldsymbol{v'}\right ) \boldsymbol{\cdot }\left (\boldsymbol{\nabla} _{\boldsymbol{x}} \mathcal{P} - \boldsymbol{\nabla} _{\boldsymbol{x}} \boldsymbol{u}^{\infty } \boldsymbol{\cdot }\boldsymbol{\nabla} _{\boldsymbol{v'}} \mathcal{P}\right ) + \frac {\boldsymbol{F}^{\textit{ext}}}{m} \boldsymbol{\cdot }\boldsymbol{\nabla} _{\boldsymbol{v'}} \mathcal{P} \nonumber \\ = \boldsymbol{\nabla} _{\boldsymbol{v'}} \boldsymbol{\cdot } \left\{\left [f \, \boldsymbol{S}(\boldsymbol{v'})\right ] \, \mathcal{P} + D \, \boldsymbol{\nabla} _{\boldsymbol{v'}} \mathcal{P} \right\}. \end{align}

(The letter C preceding the equation number denotes the corrected version.)

The analysis that follows equation 3.4 in the paper was performed using the correct equation (as it appears here), and hence remains unaffected.

References

Toppaladoddi, S. 2025 A viscous continuum theory of sea ice motion based on stochastic floe dynamics. J. Fluid Mech. 1014, A6.10.1017/jfm.2025.10279CrossRefGoogle Scholar